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Effect of live fences of Gliricidia sepium on CO 2 fluxes in tropical livestock systems
Author(s) -
VillanuevaLópez G.,
CasanovaLugo F.,
MartínezZurimendi P.,
Parsons D.,
AguilarSolís L. A.
Publication year - 2016
Publication title -
soil use and management
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.709
H-Index - 81
eISSN - 1475-2743
pISSN - 0266-0032
DOI - 10.1111/sum.12311
Subject(s) - gliricidia sepium , environmental science , relative humidity , dry season , wet season , topsoil , seasonality , hydrology (agriculture) , atmospheric sciences , diurnal temperature variation , soil water , agronomy , soil science , ecology , geography , biology , meteorology , geotechnical engineering , geology , engineering
Live fences have the potential to improve microclimatic conditions, moderate soil CO 2 fluxes and function as carbon sinks. We quantified variation in soil CO 2 fluxes from livestock silvopastoral systems under the canopies of live fences (LF), formed by Gliricidia sepium trees, or artificial fences (AF). We determined the responses of soil CO 2 fluxes to environmental factors, including diurnal and seasonal variations in temperature and relative humidity in each fencing system. Measurements were made from April to June (dry season) and from July to September (rainy season), 2012. Fluxes were similar between the two livestock systems; LF emitted 1.00 μmol CO 2 /m 2 /s and AF 1.02 μmol CO 2 /m 2 /s. Soil temperatures at 5 cm depth were 3% warmer in AF than in LF, and relative humidity was 16% greater in LF than in AF. Seasonal variation in temperature greatly affected soil CO 2 fluxes, which changed seasonally in parallel with temperature of the topsoil and relative humidity at 1 m height, peaking in late summer. Fluxes in LF and AF were greater in the rainy season (1.1 μmol CO 2 /m 2 /s, for both systems), when soil temperature was cooler and relative humidity was greatest, than during the dry season (0.9 μmol CO 2 /m 2 /s, for both systems). Soil fluxes were larger at night (00:00–06:00 h), when soil temperature was cooler and relative humidity greater, than during the morning (6:00–12:00 h), when soil temperature was warmer and relative humidity was less. The presence of G. sepium trees in LF did not influence soil CO 2 fluxes.